This section shows the main steps that have been applied to pre-process the raw data.
The CDOM spectra were modeled according to the information in Babin 2003.
acdom spectra were re-fitted using the complete data (i.e. between 350-500 nm) because the data in all_abs_transpose.txt started at 380 nm.Average background values calculated between 683-687 nm and subtracted from each spectra.
Some files were in binary format, so I could not open them (ex.: C2001000.YSA).
Some spectra start at 300 nm while others at 350 nm.
Calculated the correlation between the measured and the fitted values.
Exported the complete spectra (350-700 nm): both the raw and the modeled data.
Ed, Eu, Kd, Ku). I have cleaned the data by setting these negative values to NA.NA.DOC, AQY) from Massimo 2000.Eu means that Eu0- was estimated (see with Marcel, I do not remember what it means).
Ed is Ed0- calculated from 0.94 x ed0+.
ed to ed0-.The data is a mix of temporal and spatial observations, so how should we present the data?
By area?
Just some graphs to visualize the data. Note that the same color palette will be used to represent the areas in all graphics.
There is a total of 424 different stations that were sampled during the COASTLOOC expeditions.
C2001000, C2002000.Just an overview of the available variables (excluding radiometric measurements).
Overview of the averaged absorption spectra for each area.
Comparing acdom443 for the different areas shows that there is a clear open to coastal gradient.
We can see that the DOC follows the same pattern as acdom443.
We can also use scatter-plots to further explore the relationships among variables.
Relationships between some pigments.